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Surface water chemistry of burned and undisturbed watersheds on the Boreal Plain: an ecoregion approach
Abstract
The water chemistry of the euphotic zone in 12 lakes within burned and reference watersheds on Alberta's Boreal Plain was surveyed two years post-fire. Five burned and four reference lakes were located in the Boreal Foothills (mean elevation = 1048 m) and three reference lakes were situated at lower elevations in the Boreal Mixedwood ecoregion (748 m). Mean dissolved organic carbon (DOC) concentration in lake water from burned watersheds was 1.4-fold higher than in lake water from reference Foothills watersheds, whereas lake colour increased with the area of catchment burned divided by lake volume (r = 0.98). Reference Mixedwood lakes had higher mean total phosphorus (TP, 1.8-fold) and chlorophyll a (chl a; 4.4-fold) concentrations than reference Foothills lakes. Ten additional lakes from a previous study in boreal Alberta were used to further compare water chemistry between ecoregions. Boreal Mixedwood lakes (n = 13) had higher TP (2.3-fold), chl a (3-fold), and Ca2+ + Mg2+ (3.3-fold) concentrations than Boreal Foothills lakes (n = 9). Our data suggest an influence of forest fire on lake chemistry in the Boreal Foothills, and demonstrate the need for an ecoregion approach to detect the impacts of watershed disturbance on the Boreal Plain. Key words: watershed disturbance, forest fire, lake nutrients, lake elevation, phosphorus, chlorophyll a, anions, cations, dissolved organic carbon.
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One study of conductivity in lakes exhibited a decline post-fire.
“We encountered one study of conductivity in lakes which exhibited a decline post-fire (Allen et al., 2003).”
From Wildfire Induces Changes in Receiving Waters: A Review With Considerations for Water Quality Management (2022) · cites this paper as Allen et al., 2003
At least some organic carbon increases in aquatic ecosystems below burned watersheds, especially lakes, are likely attributable to algae.
“At least some organic carbon increases in aquatic ecosystems below burned watersheds, especially lakes, are likely attributable to algae.”
From Wildfire Induces Changes in Receiving Waters: A Review With Considerations for Water Quality Management (2022) · cites this paper as Allen et al., 2003
Alkalinity decreases in boreal regions have been attributed both to peatland release of hydrogen ions as well as oxidation of reduced sulfur.
“and this has been attributed both to peatland release of hydrogen ions as well as oxidation of reduced sulfur (Allen et al., 2003; Bayley et al., 1992; Crilly et al., 2017; Lydersen et al., 2014).”
From Wildfire Induces Changes in Receiving Waters: A Review With Considerations for Water Quality Management (2022) · cites this paper as Allen et al., 2003
Algal biomass in downstream lakes, especially oligotrophic lakes, often increased in response to dissolved nutrient export from burned watersheds and contributed organic carbon through exudation or lysis.
“Algal biomass in these downstream lakes, especially oligotrophic lakes, often increased in response to dissolved nutrient export from burned watersheds and contributed organic carbon through exudation or lysis (Allen et al., 2003, 2005; McCullough et al., 2019).”
From Wildfire Induces Changes in Receiving Waters: A Review With Considerations for Water Quality Management (2022) · cites this paper as Allen et al., 2003
In some lakes, the effect of nutrient enrichment on algal biomass could be dampened by decreased light availability from post-fire dissolved or suspended material.
“Some studies of lakes, however, have shown this effect could be dampened by decreased light availability from post-fire dissolved or suspended material (e.g., Allen et al., 2003).”
From Wildfire Induces Changes in Receiving Waters: A Review With Considerations for Water Quality Management (2022) · cites this paper as Allen et al., 2003
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Paul, M. J., LeDuc, S. D., Lassiter, M. G., Moorhead, L. C., Noyes, P. D., & Leibowitz, S. G. (2022) · Water Resources Research · doi:10.1029/2021wr030699 · Cited by 241
“Some studies of lakes, however, have shown this effect could be dampened by decreased light availability from post-fire dissolved or suspended material (e.g., Allen et al., 2003).”
Influential
Metadata
- Authors
- Allen, E. W., Prepas, E. E., Gabos, S., Strachan, W., & Chen, W.
- Venue
- Journal of Environmental Engineering and Science
- Publisher
- Emerald
- Published
- 2003-06-01
- Volume
- 2
- Issue
- Supplement 1
- Pages
- S73-S86
- ISSN
- 1496-2551 (ISSN-L)
- 1496-256X
- OpenAlex
- W2019597333
- Cited by
- 27
- References
- 0
- Citations by year
- 2026: 1 · 2025: 4 · 2024: 2 · 2023: 2 · 2022: 3 · 2021: 1 · 2020: 2 · 2019: 2 · 2018: 1 · 2016: 1 · 2013: 2
- FWCI
- 1.06
- Type
- journal article
- Language
- en
- Open access
- closed
- Locations
- Journal of Environmental Engineering and Science (publishedVersion)
- Topics
- Physical Sciences › Environmental Science › Global and Planetary Change › Fire effects on ecosystems
- Physical Sciences › Environmental Science › Environmental Chemistry › Aquatic Ecosystems and Phytoplankton Dynamics
- Physical Sciences › Environmental Science › Water Science and Technology › Water Quality and Resources Studies
- Keywords
- burned watersheds, surface water chemistry, lake nutrients, dissolved organic carbon, phosphorus, chlorophyll a, ecoregions, boreal mixedwood forest, watershed disturbance, post-fire recovery
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